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Modeling the interaction between the solar wind and Saturn’s magnetosphere by the AMR-CESE-MHD method

机译:通过AMR-CESE-MHD方法模拟太阳风与土星磁层之间的相互作用

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In this paper, the space-time conservation element and solution element (CESE) method in general curvilinear coordinates is successfully applied to the three-dimensional magnetohydrodynamic(MHD) simulations of the interaction between the solar wind and Saturn’s magnetosphere on a six-component grid system. As a new numerical model modified for the study of the interaction between the solar wind and Saturn’s magnetosphere, we obtain the large-scale configurations of Saturn’s magnetosphere under the steady solar wind with due southward interplanetary magnetic field (IMF) conditions. The numerical results clearly indicate that the global structure of Saturn’s magnetosphere is strongly affected by the rotation of Saturn as well as by the solar wind. The subsolar standoff distances of the magnetopause and the bow shock in our model are consistent with those predicted by the data-based empirical models. Our MHD results also show that a plasmoid forms in the magnetotail under the effect of the fast planetary rotation. However, somewhat differently from the previous models, we find that there are two flow vortices generated on the duskside under due southward IMF at Saturn. On the duskside, the clockwise one closer to the planet is excited by the velocity shear between the rotational flows and the sunward flows, while the anticlockwise one is generated from the velocity shear between the tailward flows along the magnetopause and the sunward flows.
机译:本文将一般曲线坐标系中的时空守恒元素和解元素(CESE)方法成功应用于六分量网格上太阳风与土星磁层相互作用的三维磁流体动力学(MHD)模拟系统。作为用于研究太阳风与土星磁层之间相互作用的新的数值模型,我们获得了在稳定的太阳风和适当的向南行星际磁场(IMF)条件下,土星磁层的大规模配置。数值结果清楚地表明,土星磁层的整体结构受到土星自转以及太阳风的强烈影响。在我们的模型中,磁层顶和弓形冲击的次太阳距离距离与基于数据的经验模型所预测的距离一致。我们的MHD结果还表明,在快速行星旋转的影响下,磁尾中会形成等离子体。但是,与以前的模型有些不同,我们发现在土星正下方的IMF向南下,在黄昏侧产生了两个流动涡流。在黄昏时,更靠近行星的顺时针方向是由旋转流和向阳流之间的速度剪切所激发,而逆时针方向是由沿磁层顶和向后流的向后流之间的速度剪切产生的。

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